Surface Layer Accretion in Conventional and Transitional Disks Driven by Far-Ultraviolet Ionization

Details Surface Layer Accretion in Conventional and Transitional Disks Driven by Far-Ultraviolet Ionization Surface Layer Accretion in Conventional and Transitional Disks Driven by Far-Ultraviolet Ionization

2011-04-12

arxiv.org/abs/1104.2320v2

Astronomy and Astrophysics

Astrophysics

Earth and Planetary Astrophysics

Final proofed version. Corrects X-ray-driven accretion rates in the high PAH case for Figures 8 and 9

Scientific paper

Whether protoplanetary disks accrete at observationally significant rates by the magnetorotational instability (MRI) depends on how well ionized they are. Disk surface layers ionized by stellar X-rays are susceptible to charge neutralization by small condensates, ranging from ~0.01-micron-sized grains to angstrom-sized polycyclic aromatic hydrocarbons (PAHs). Ion densities in X-ray-irradiated surfaces are so low that ambipolar diffusion weakens the MRI. Here we show that ionization by stellar far-ultraviolet (FUV) radiation enables full-blown MRI turbulence in disk surface layers. Far-UV ionization of atomic carbon and sulfur produces a plasma so dense that it is immune to ion recombination on grains and PAHs. The FUV-ionized layer, of thickness 0.01--0.1 g/cm^2, behaves in the ideal magnetohydrodynamic limit and can accrete at observationally significant rates at radii > 1--10 AU. Surface layer accretion driven by FUV ionization can reproduce the trend of increasing accretion rate with increasing hole size seen in transitional disks. At radii < 1--10 AU, FUV-ionized surface layers cannot sustain the accretion rates generated at larger distance, and unless turbulent mixing of plasma can thicken the MRI-active layer, an additional means of transport is needed. In the case of transitional disks, it could be provided by planets.

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